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  • 1
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    Elastische Eigenschaften von Gesteinen und Mineralien (1952)
    Springer
    In:  Professional Paper, Landolt Börnstein (6. Edition) III. Band: Astronomie und Geophysik, Berlin, Springer, vol. 7, no. XVI:, pp. 326-330, (ISBN: 3-540-23712-7)
    Details
    Publication Date: 1952
    Keywords: Elasticity ; Rock mechanics ; Physical properties of rocks
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Seismizität der Erde (1952)
    Springer
    In:  Professional Paper, Landolt Börnstein (6. Edition) III. Band: Astronomie und Geophysik, Berlin, Springer, vol. 7, no. XVI:, pp. 369-375, (ISBN: 3-540-23712-7)
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    Publication Date: 1952
    Keywords: Seismology ; Seismicity
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Erdbebenwellen (1952)
    Springer
    In:  Professional Paper, Landolt Börnstein (6. Edition) III. Band: Astronomie und Geophysik, Berlin, Springer, vol. 7, no. XVI:, pp. 375-384, (ISBN: 3-540-23712-7)
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    Publication Date: 1952
    Keywords: Seismology ; Waves
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
    Electronic Resource
    Electronic Resource
    Deep-focus earthquakes in the Mediterranean region (1948)
    Springer
    Pure and applied geophysics 12 (1948), S. 130-133 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Zusammenfassung In Tabelle I geben die Verff. eine Liste der ihnen bekannten Tiefenbeben im östlichen Mittelmeer. Fig. 1 zeigt, dass deren IIerde im Allgemeinen in den Zonen der tätigen Vulkane liegen, ähnlich wie in der Umgebung des Pazifischen Ozeans. Dagegen ist deren Zusammenfallen mit positiven Schwereanomalien weniger doutlich.
    Abstract: Riassunto Gli AA. hanno raccolto nella Tab. 1 l'elenco dei terremoti profondi a loro noti del bacino mediterraneo orientale. La Fig. 1 mostra che in generale gli epicentri relativi sono distribuiti nelle zone dei vulcani attivi, analogamente a quanto accade ne'le regioni dell'Oceano Pacifico. Per contro, la connessione con le anomalie gravimetriche positive risulta meno evidente.
    Notes: Summary In Table I the authors give a list of known deep-focus earthquakes in the eastern Mediterranean. Fig. 1 shows that their epicenters generally lie in the zones of active volcanoes, as in the regions surrounding the Pacific Ocean; however, their coincidence with positive gravity anomalies is less evident.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02332102
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  • 5
    Electronic Resource
    Electronic Resource
    Effects of low-velocity layers (1954)
    Springer
    Pure and applied geophysics 29 (1954), S. 1-10 
    Details
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary Effects of low-velocity channels in the atmosphere, the ocean and the solid earth are discussed. There are two major low-velocity channels in the atmosphere, one with its axis at the tropopause, and another at a height of about 80 km. They produce “zones of silence” and permit the transmissions of waves involving the whole atmosphere. Low-velocity layers in the ocean result from the combined effects of temperature, pressure and salinity. In the earth, the sudden decrease of velocity at the boundary of the core produces a low-velocity at the boundary of the core produces a low-velocity channel for elastic waves. In the earth's crust there are two major low velocity shannels, one below theMohorovičić discontinuity, the other at a depth of about 15 Km. Misinterpretation of their effects has caused incorrect conclusions concerning the structure of the outer portion of the earth's mantle.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01988601
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  • 6
    Electronic Resource
    Electronic Resource
    Neue Ergebnisse über den Aufbau der Erde (1956)
    Springer
    International journal of earth sciences 45 (1956), S. 342-353 
    Details
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Zusammenfassung In den letzten Jahren haben sich viele unserer Anschauungen über den Aufbau der Erde erheblich geändert. Neue Ergebnisse, besonders durch Laboratoriumsexperimente und auf dem Gebiete der Erdbebenforschung, haben gezeigt, daß vielfach Folgerungen, die als gesicherte Ergebnisse betrachtet worden waren, auf zu einfache Annahmen aufgebaut waren. Im folgenden werden einige der neuen Beobachtungen und Ansichten besprochen.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01802020
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  • 7
    Electronic Resource
    Electronic Resource
    Zur Frage der Gebirgswurzeln (1957)
    Springer
    International journal of earth sciences 46 (1957), S. 30-38 
    Details
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Roots of mountains are studied by use of gravimetric data, dispersion of surface waves, travel times of refracted and reflected body waves from earthquakes or artificial explosions. Under Southern and Central California, the thickness of the crust (depth of the Mohorovičić discontinuity) increases from about 20 km near the coast to 30–35 km under the lower valleys and to about 50 km under the Sierra Nevada. Near the Atlantic coast of the United States it increases from about 20 km under the shelf to about 30 km under the coast, 35 km under the Canadian Shield, and about 45 km under the southern Appalachians. In Western Europe it is about 25–30 km, seems to increase under the Central and Southern Alps to 45–50 km and possibly to 60 km under the Abruzzi. The thickness of the „granitic“ layer seems to be 25–30 km under Southern California and the Sierra Nevada, roughly 20 km under western Europe, but seems to increase to about 35 km under the Central and Southern Alps. Thus, the root under the Sierra Nevada is possibly mainly an effect of a thickening of the „basaltic“ layer, while under the Alps it results mainly from a thicker „granitic“ layer. This difference could result from different tectonic processes in the two regions during their late geological history. The local temperatures in the earth's crust can apparently greatly affect the depth at which phase changes occur and thus the thickness of the crust. Processes connected with reestablishment of isostatic equilibrium probably occur mainly below the crust.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01802881
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  • 8
    Electronic Resource
    Electronic Resource
    Postglacial uplift in the Great Lakes region (1954)
    Springer
    Meteorology and atmospheric physics 7 (1954), S. 243-251 
    Details
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Zusammenfassung Neue Ergebnisse über die Geländehebung im nördlichen Nordamerika und in Fennoskandien werden zusammen mit früheren Ergebnissen diskutiert. Die weitaus beste Erklärung bietet die Hypothese, daß die Hebung in beiden Gebieten durch Fließbewegungen in der Erdkruste verursacht wird mit der Tendenz, das isostatische Gleichgewicht wiederherzustellen, das durch das Abschmelzen der während der Eiszeit angehäuften Eismassen gestört worden war. Die wesentlichen für diese Hypothese in Frage kommenden Größen sind in beiden Gebieten von der gleichen Größenordnung. Trotzdem wird diese Hypothese in mehreren Veröffentlichungen für die gegenwärtige Landhebung in Nordamerika abgelehnt, während sie für die Hebung in Fennoskandien mit ganz wenigen Ausnahmen angenommen wird, wofür Gründe diskutiert werden.
    Abstract: Résumé L'auteur discute les anciens et les nouveaux résultats des recherches concernant les mouvements ascendants du sol dans le nord de l'Amérique septentrionale et en Fennoscandie. La meilleure explication en est fournie par l'hypothèse que ces phénomènes sont provoqués par des courants à l'intérieur de l'écorce terrestre tendant à rétablir l'équilibre isostatique, qui avait été rompu par la fonte des glaces diluviales. Les éléments entrant en ligne de compte sont du même ordre de grandeur pour les deux régions. Malgré cela, la même hypothèse, généralement admise en ce qui concerne la Fennoscandie, est rejetée, dans plusieurs publications, pour l'Amérique du Nord, en partie à la suite de l'interprétation erronée de certaines données.
    Notes: Summary New data concerning the uplift in northern North America and in Fennoscandia are combined with earlier findings. The main quantities involved in the hypothesis of postglacial uplift are of the same order of magnitude for Fennoscandia and for the Great Lakes-Hudson Bay regions. Whereas the hypothesis of postglacial uplift is readily accepted for Fennoscandia, it has been rejected in several publications for the present uplift in North America, partly as a consequence of misinterpretation of data. Actually, it offers the best explanation by far for the uplift in both areas.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02277920
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  • 9
    Electronic Resource
    Electronic Resource
    Die Geschwindigkeit der Erdbebenwellen und die elastischen Konstanten in den obersten Erdschichten (1925)
    Springer
    Naturwissenschaften 13 (1925), S. 360-362 
    Details
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01559126
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  • 10
    Electronic Resource
    Electronic Resource
    Besprechungen (1929)
    Springer
    Naturwissenschaften 17 (1929), S. 933-942 
    Details
    ISSN: 1432-1904
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01506587
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